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Stability of carbonate minerals in a hydrous mantle

Year Book - Carnegie Institution of Washington 75): 631-636

Stability of carbonate minerals in a hydrous mantle

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Accession: 020083431

Related references

Shibata Takeo; Nguyen Jeffrey H.; Jeanloz Raymond; Ohtani Eiji, 1996: Stability of hydrous minerals in the mid-mantle. Eos, Transactions, American Geophysical Union 77(17, Suppl

Ohtani E.; Mizobata H.; Kubo T., 1999: Stability of high pressure hydrous minerals in the Earth's interior and the mantle dynamics. Mineralogical Journal 21(1): 33-34

Eggler D.H., 1978: Stability of dolomite in a hydrous mantle, with implications for the mantle solidus. Geology (Boulder) 6(7): 397-400

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Pamato, M.G.; Boffa Ballaran, T.; Frost, D.J.; Kurnosov, A.; Trots, D.M., 2011: The elasticity of hydrous minerals in the lower mantle. Water is recycled into the Earth's interior by hydrous minerals in descending slabs and the amount of water that is transported into the deep mantle depends on the stability of high-pressure hydrous phases. As water plays an important role in...

Basu A.R., 1978: Trace elements and Sr-isotopes in some mantle-derived hydrous minerals and their significance. New analyses of K, Rb, Sr and Ba contents and the 87Sr86Sr ratios of eight amphiboles, one phlogopite, two diopsides and one host alkalic basalt for an amphibole are reported: The samples are mostly inclusions in alkalic basalts and occur in assoc...

Wang, J.; Bass, J.D., 2011: Elastic properties of hydrous and anhydrous mantle minerals at high pressure. Anyhdrous and hydrous forms of wadsleyite and ringwoodite, high-pressure phases of (Mg,Fe)2 SiO4 +- H2 O, are major constituents of the transition zone of Earth's mantle, and are likely abundant in many subducting slabs. Therefore, the seismi...

L.R.; Hemley R.J.; Mao H.K.; Carr G.L.; Williams G.P., 1996: Synchrotron micro-infrared spectroscopy; applications to hydrous mantle minerals. Eos, Transactions, American Geophysical Union 77(46, Suppl

Frost Daniel J., 2006: The stability of hydrous mantle phases. Reviews in Mineralogy and Geochemistry 62: 243-271

Ken-Ichiro Aoki; Satoshi Kanisawa, 1979: Fluorine contents of some hydrous minerals derived from upper mantle and lower crust. Fluorine contents have been determined in about forty samples of amphibole, mica and apatite in alkali basalt and kimberlite and their incorporated xenoliths. They show a wide variation ranging from 15,000 to 100 ppm, corresponding to about 40 to...